Crustal seismic velocity responds to a magmatic intrusion and seasonal loading in Iceland's Northern Volcanic Zone.

Seismic noise interferometry is an exciting technique for studying volcanoes, providing a continuous measurement of seismic velocity changes (dv/v), which are sensitive to magmatic processes that affect the surrounding crust. However, understanding the exact mechanisms causing changes in dv/v is oft...

Full description

Bibliographic Details
Main Authors: Donaldson, C, Winder, T, Caudron, C, White, R S
Format: Text
Language:unknown
Published: Apollo - University of Cambridge Repository 2019
Subjects:
Online Access:https://dx.doi.org/10.17863/cam.47555
https://www.repository.cam.ac.uk/handle/1810/300483